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Libros sobre el tema "Natural limestone"

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Publicado: 1 de junio de 2024

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1

Tabin Limestone Scientific Expedition (2000). Tabin Limestone Scientific Expedition, 2000: [papers]. Kota Kinabalu: Universiti Malaysia Sabah, 2003.

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2

Windrum, Andrew. Lincolnshire and Rutland Limestone natural area profile. Peterborough: English Nature, 1997.

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3

Windrum, Andrew. Lincolnshire and Rutland Limestone natural area profile. Peterborough: English Nature, 1997.

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4

America, Marble Institute of, ed. Natural stone: Marble, onyx, travertine, granite, quarzite, limestone. 6a ed. Firenze: Studio Marmo, 2005.

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5

Gillham, Mary E. Limestone downs: Commons, farms and woods. Bridgend: Glamorgan Wildlife Trust, 1991.

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6

Hnyk, Peter. Skály a lidé. Červený Kostelec: Pavel Mervart, 2019.

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7

Gallagher, Teresa Clark. The natural history of Pierrepont State Park and Limestone Preserve, Ridgefield, Connecticut. [Ridgefield, Conn: Town of Ridgefield Conservation Commission, 1991.

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8

Wickstrom, Lawrence H. Stratigraphy, structure, and production history of the Trenton Limestone (Ordovician) and adjacent strata in northwestern Ohio. Columbus: State of Ohio, Dept. of Natural Resources, Division of Geological Survey, 1992.

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9

Wolfgang, Tegethoff F., Rohleder Johannes y Kroker Evelyn, eds. Calcium carbonate: From the Cretaceous period into the 21st century. Basel: Birkhäuser Verlag, 2001.

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10

John, Graves. From a limestone ledge: Some essays and other ruminations about country life in Texas. Houston: Gulf Pub. Co., 1991.

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11

John, Graves. From a limestone ledge: Some essays and other ruminations about country life in Texas. Dallas: Southern Methodist University Press, 2004.

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12

Stith, David A. Supplemental core investigations for high-calcium limestones in western Ohio and discussion of natural gas and stratigraphic relationships in the Middle to Upper Ordovician rocks of southwestern Ohio. Columbus: State of Ohio, Dept. of Natural Resources, Division of Geological Survey, 1986.

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13

Amorim, Laurindo. Lisboa Metropolitan Area and the Lioz Limestone Selection Environmental Influence: From Natural to Artificial Limestone. Independently Published, 2020.

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14

LaMoreaux, James W., Catherine Bertrand, Jacques Mudry y François Zwahlen. H2Karst Research in Limestone Hydrogeology. Springer London, Limited, 2014.

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15

H2Karst Research in Limestone Hydrogeology. Springer International Publishing AG, 2014.

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16

Boobalan, A. Janarthana. Limestone Caves: Monograph on One of the Natural Wonder. Independently Published, 2021.

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17

Burren Country Travels Through An Irish Limestone Landscape. Collins Press, 2011.

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18

Clements, Paul. Burren Country: Travels Through an Irish Limestone Landscape. M.H. Gill & Co. U. C., 2011.

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19

Harrington, M. G. Characteristics of 1-year-old natural pinyon seedlings. 1987.

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20

Bell, James Robert. Habitat use, community structure and biogeography of spiders (araneae) in semi-natural and disturbed limestone grassland. 1999.

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21

Rapid and participatory biodiversity assessments (BIORAP) in Khammouan Limestone National Biodiversity Conservation Area, Khammouan Province, Lao PDR: Final report. [Pathim Thānī]: WWF-Thailand Project Office, 1998.

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22

Feldman, Howard R. Brachiopods of the Onondaga Limestone in Central and Southeastern New York (Bulletin of the American Museum of Natural History, Vol 179, Article 3). Amer Museum of Natural History, 1985.

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23

Rohleder, J. y E. Kroker. Calcium Carbonate: From the Cretaceous Period into the 21st Century. Birkhauser, 2002.

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24

Rohleder, J., E. Kroker y F. Wolfgang Tegethoff. Calcium Carbonate: From the Cretaceous Period into the 21st Century. Springer Basel AG, 2014.

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25

Cronin, Mikel. Spearfish Canyon: And Other Black Hills Limestone. Sharp End Publishing, LLC, 2011.

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26

Algaze, Guillermo y Timothy Matney. Titriş Höyük: The Nature and Context of Third Millennium B.C.E. Urbanism in the Upper Euphrates Basin. Editado por Gregory McMahon y Sharon Steadman. Oxford University Press, 2012. http://dx.doi.org/10.1093/oxfordhb/9780195376142.013.0046.

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This article discusses findings from excavations at Titriş Höyük. At the time of its foundation as an urban center in the Middle Early Bronze Age, Titriş Höyük possessed the combined advantages of locally available timber, multiple perennial water sources and associated year-round cultivable floodplains suited to garden crops, and broad, rain-fed arable tracts suited to grain cultivation. Additionally, the site was surrounded by gentle limestone hills well suited to viticulture and livestock grazing. However, this benign framework provided a necessary but not sufficient condition for the development of the site. The sufficient condition was the city's location along the road to the Samsat ford, which made it a natural arbiter of a portion of long-distance east–west trade across the northern fringes of “Greater Mesopotamia” in the third millennium—a fact attested by the number and variety of imports found in excavated mortuary and domestic contexts across the city.
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27

Sheppard, Charles R. C., Simon K. Davy, Graham M. Pilling y Nicholas A. J. Graham. Coral reefs. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780198787341.003.0001.

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Coral reefs are the ocean’s richest ecosystem in terms of biodiversity and productivity. They are restricted to tropical waters, where conditions of salinity, temperature and sedimentation are suitable. Where they grow, their main benthic organisms deposit substantial limestone skeletons, such that they effectively make their own habitat which sustains their dynamic nature and supports the wide range of species which inhabit them. Reefs grow to the low tide level, thus providing a breakwater, but the richest parts lie 5–20 metres below the surface, an area where light is still sufficient but where sediment and turbulence are not severe. Reefs may occur as narrow fringing reefs bordering a continental coast, as huge offshore barrier reefs or as series of atolls that support entire nations; the biogenic nature of corals is enormously important to mankind.
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28

Resource management in limestone landscapes: International perspectives : proceedings of the International Geographical Union, Study Group Man's Impact on Karst, Sydney, 15-21 August 1988. Canberra, Australia: Dept. of Geography & Oceanography, University College, Australian Defence Force Academy, 1989.

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29

Martin, Derek y Peter Stacey, eds. Guidelines for Open Pit Slope Design in Weak Rocks. CSIRO Publishing, 2018. http://dx.doi.org/10.1071/9781486303489.

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Weak rocks encountered in open pit mines cover a wide variety of materials, with properties ranging between soil and rock. As such, they can provide a significant challenge for the slope designer. For these materials, the mass strength can be the primary control in the design of the pit slopes, although structures can also play an important role. Because of the typically weak nature of the materials, groundwater and surface water can also have a controlling influence on stability. Guidelines for Open Pit Slope Design in Weak Rocks is a companion to Guidelines for Open Pit Slope Design, which was published in 2009 and dealt primarily with strong rocks. Both books were commissioned under the Large Open Pit (LOP) project, which is sponsored by major mining companies. These books provide summaries of the current state of practice for the design, implementation and assessment of slopes in open pits, with a view to meeting the requirements of safety, as well as the recovery of anticipated ore reserves. This book, which follows the general cycle of the slope design process for open pits, contains 12 chapters. These chapters were compiled and written by industry experts and contain a large number of case histories. The initial chapters address field data collection, the critical aspects of determining the strength of weak rocks, the role of groundwater in weak rock slope stability and slope design considerations, which can differ somewhat from those applied to strong rock. The subsequent chapters address the principal weak rock types that are encountered in open pit mines, including cemented colluvial sediments, weak sedimentary mudstone rocks, soft coals and chalk, weak limestone, saprolite, soft iron ores and other leached rocks, and hydrothermally altered rocks. A final chapter deals with design implementation aspects, including mine planning, monitoring, surface water control and closure of weak rock slopes. As with the other books in this series, Guidelines for Open Pit Slope Design in Weak Rocks provides guidance to practitioners involved in the design and implementation of open pit slopes, particularly geotechnical engineers, mining engineers, geologists and other personnel working at operating mines.
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30

Skupio, Rafał. Zastosowanie nieinwazyjnych pomiarów rdzeni wiertniczych do zwiększenia informacji na temat parametrów skał zbiornikowych. Instytut Nafty i Gazu - Państwowy Instytut Badawczy, 2022. http://dx.doi.org/10.18668/pn2022.237.

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The research carried out in the monograph aimed to create a measurement and interpretation system which is to obtain reliable results of well logging with the accuracy of laboratory measurements. Continuous core measurements allow for the generation of logging results without the impact of the borehole and facilitate the depth matching of the core to well log data. Four main chapters can be distinguished in this work: research methodology with a description of the devices used; partial results of core measurements made on various types of rocks; a proposal for a research system, and comprehensive data interpretation for selected boreholes. The methodological part concerned the description of the equipment for continuous measurements of cores in the field of natural gamma radioactivity (K, U, Th) with the application for bulk density measurements using the gamma-gamma method, X-ray fl uorescence spectrometers (XRF) for measuring the chemical composition of rocks and computed tomography (CT) for imaging of the core structure as well as determination of radiological density in Hounsfi eld units (HU). Rock studies were carried out on material representing formations of diff erent lithologies, such as shales, sandstones, limestones, dolomites, anhydrite, siltstones and heterolithic sandstone-siltstone-claystone complexes. The results of measurements made using individual methods have been described in detail and compared with the results of laboratory measurements and well logging data. Test measurements with data processing and interpretation were made on the cores from five boreholes (T-1, O-4, Pt-1, L-7, P-5H), whereas a comprehensive interpretation of the results was carried out for three other boreholes (J-1, P-4, T-2). The new methodology of spectral gamma measurements made it possible to obtain precise concentrations of potassium, uranium and thorium in rocks with high and low radioactivity. The results made it possible to standardise the archival gamma-ray logs made with the Russian-type probes from imp/min to API standard units and to obtain data on the content of K, U, and Th in the core intervals. Using the Cs-137 source in the device for the gamma equipment made it possible to carry out measurements of the bulk density in g/cm3 units. The lithological interpretation based on XRF measurements and mineralogical-chemical models allowed to obtain logs with increased resolution and a more signifi cant number of minerals than was the case with the interpretation of the well logging. In addition, it has been shown that the XRF measurement methodology can be used during the geosteering procedure. The results of the core tests using the CT computed tomography method were presented in combined images and continuous curves of density in HU units. The experience and the presentation of the full scope of measurement and interpretation workflow allowed to propose a procedure for conducting a full range of analyses, considering various types of material provided for research. The procedure considers the full range of analyses as well as the measurements of selected parameters depending on the client’s needs. Keywords: petrophysics, core analyses, XRF spectrometry, computed tomography, gamma profiling, lithological interpretation
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